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《Acta Scicentiarum Naturalum Universitis Pekinesis》 1990-04
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Application of the Carbon Stable Isotope to the Long-range Stratigraphic Correlation of the Devonian- Carboniferous and Frasnian-Famennian Boundary Beds

BAI Shunliang (Department of Geology, Beijing University)WANG Darui, JANG Jiajian (Institute of Petroleum Exploration and Development)  
The D-C boundary shale below the Siphonodella sulcata Zone of Huangmao Section, Guangxi, and Muhua Section, Guizhou reveal negative perturbation ofδ13C values of 17‰ and 13‰ respectively. Correlation between Huangmao Section and Muhua Section based on conodont succession can be well confirmed by the δ13C value curves. At Nandong Section, Guangxi, within the Palmatolepis linguiformis Zone (i. e. Uppermost gigas Zone)of the uppermost Frasnian, there are three horizons revealing δ13C negative perturbation, the lowest one is of 6‰. The Nandong Section bear pelagic fossils, and the F-F boundary can be well defined by the extinction of the conodont species Palmatolepis gigas, Pa. linguiformis and the first occurence of Pa. triangularis which was recommended by the Subcommission on Devonian Stratigraphy as the marker of the base of the Famennian. The Xikuangshan Section, Hunan, bear neritic fossils and lacks marker species. It is assumed that the F-F boundary should be placed at the level above the mass extinction line of reef corals and bryozoa, beneath the first occurence of neritic conodont species Icriodus deformatus Han. Thus the F-F boundaries of Nandong and Xikuangshan are correlated roughly by indirect biostratigraphic method which needs collateral evidence. The biostratigraphic result can be elaborated by the δ13C data. The extinction line of the reefs at Xikuangshan is somewhat lower than the F-F boundary defined by the conodonts at Nandong. The δ13C fluctuation curve of the F-F boundary has prominent feature, that under certain condition it has the potentiality for long-range correlation.
【Fund】: 国家自然科学基金会;; 国家教委科学技术基金会
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